Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic 14C Trapped in Polar Ice

被引:0
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作者
BenZvi, Segev [1 ]
Petrenko, Vasilii V. [2 ]
Hmiel, Benjamin [2 ]
Dyonisius, Michael [2 ]
Smith, Andrew M. [3 ]
Yang, Bin [3 ]
Hua, Quan [3 ]
机构
[1] Univ Rochester, Dept Phys & Astron, Rochester, NY 14627 USA
[2] Univ Rochester, Dept Earth & Environm Sci, Rochester, NY USA
[3] ANSTO, Locked Bag 2001, Kirrawee DC, NSW 2232, Australia
基金
美国国家科学基金会;
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中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Carbon-14 (C-14) is produced in the atmosphere when neutrons from cosmic-ray air showers are captured by N-14 nuclei. Atmospheric C-14 becomes trapped in air bubbles in polar ice as compacted snow (firn) transforms into ice. C-14 is also produced in situ in ice grains by penetrating cosmic-ray neutrons and muons. Recent ice core measurements indicate that in the (CO)-C-14 phase, the C-14 is dominated by the in situ cosmogenic component at most ice coring sites. Thus, it should be possible to use ice-bound (CO)-C-14 to reconstruct the historical flux of cosmic rays at Earth, without the transport and deposition uncertainties associated with Be-10 or the carbon cycle uncertainties affecting atmospheric (CO2)-C-14. The measurements will be sensitive to the cosmic-ray flux above the energy range most affected by solar modulation. We present estimates of the expected sensitivity of (CO)-C-14 in ice cores to the historical flux of Galactic cosmic rays, based on recent studies of (CO)-C-14 in polar ice.
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页数:8
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